Bryce Canyon National Park is located in southern Utah, about 50 miles northeast of Zain National Park and is 1,000 feet taller. So it has a colder climate and more precipitation. An example of its similarity and proximity but higher elevation is Cedar Brex National Reserve. The highest point in Bryce National Park is the rainbow point, where the Aquarius Plateau, Bryce Amphitheatre, Henry Mountains, Red Rock Cliffs, White Rock Cliffs. It is located on the Colorado Plateau and crosses the southeast side of the Ponzagonte Plateau. Visitors usually climb the plateau and look at the valley containing faults and the Pariya River next to it. The edge of the Kaiparowitz Plateau closes the opposite side of the valley. The Aquarius Plateau, Bryce Amphitheatre, Henley Mountains, Red Rock Cliffs, White Rock Cliffs. All visible. The rock formations in Bryce National Park are beautiful, and the surface of the rock produces fire-like colors in the sunlight. Bryce Canyon is not a central water flow erosion, so it is not technically a canyon. It is a source erosion to dig out the Cenozoic strata of the Ponshagangte Plateau. This erosion of the law has become a number of delicate and colorful pointed cylindrical rocks, called rock columns, up to 200 feet. A series of open-air theaters stretched over 20 miles in the park. The largest of them is the Bryce Open-air Theatre, 12 miles long, 3 miles wide and 800 feet deep. The highest point is the rainbow point, 9,105 feet high, which is the end of the scenic corridor. At this point, the Aquarius Plateau, Bryce Amphitheatre, Henry Mountains, Red Rock Cliffs, and White Rock Cliffs can be seen. The Cope Valley, which is located in the northeast corner of the park, serves as the outlet for the park and is the park's lowest point, about 6,600 feet high.